PPT-Offshore Seismic and the Regulatory Tidal Wave

Author : aaron | Published Date : 2017-08-27

Shawn L Rice Board of Directors IAGC NOIA Annual Meeting April 20 2016 shawnriceiongeocom 5 Year Lease Plan March 15 th 5Year Plan Released 2017 2022 Excludes

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Offshore Seismic and the Regulatory Tidal Wave: Transcript


Shawn L Rice Board of Directors IAGC NOIA Annual Meeting April 20 2016 shawnriceiongeocom 5 Year Lease Plan March 15 th 5Year Plan Released 2017 2022 Excludes Leasing Offshore Atlantic. 2 Energy . Research and Development. Brian Polagye. Northwest National Marine Renewable Energy Center. Department of Mechanical Engineering. University of Washington. Alaska Hydrokinetics Technical Conference. Seismic velocities – P & S. Relationship to elastic moduli. Seismic anisotropy. . -- directional variation in seismic velocity. Seismic Attenuation – 1/. Q. p. & 1/Q. s. . -- What is seismic attenuation?. Ch. 5.4, 5.9-5.10). Phys. 105. Dr. Harris. 4/1/13. What Causes Tides?. http://www.pbs.org/wgbh/nova/earth/what-causes-the-tides.html. high tide. low tide. History of Tidal. Tidal energy is one of the oldest forms of energy used by humans. By The Tidal Washers!!!. Contents. Why do we need renewable energy?. How Tidal Energy works?. Examples and Pictures. Advantages. Disadvantages. Future. Quiz – Have you been listening carefully?. Game. Flat. Morphodynamics: . A . Synthesis. 1) On tidal flats, sediment (especially mud) moves toward areas of weaker . energy.. 2) Tides usually move sediment . landward; . waves usually move. sediment seaward.. Andrew . Chavous. & Carlo . Raiteri. Tides. Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun and the rotation of the Earth.. Glenn . Biasi. 1. , Leiph . Preston. 2. , and Ileana . Tibuleac. 1. Nevada Seismological Laboratory, University of Nevada Reno, Reno, NV 89557. 2. Sandia National Laboratory, Albuquerque, NM. Overview. Danny Hertel. EPS 109. Prof. . Militzer. Background/Method. As seismic waves travel through different mediums in the earth, the different mediums create different wave velocities. With geophones, the amplitude of the wave response can be measured at the surface and overlaid to create travel-time curves that tell what’s underneath.. ITET G. . MAGGIOLINI . & . “The green . school. network. ” . present. . What. . is. an . earthquake. ?. An earthquake (also known as a quake, . tremor) . is the . shaking of the surface. of the Earth, resulting from the sudden release of energy in the Earth's lithosphere that creates seismic waves. . Seismic . Waves. . are shock . waves . given off by earthquakes. . There are 2 types:. 1. . Body Waves. . originate from the . focus. (. F. ). travel . through. . the earth. . They’re used to locate . Core Contractors are your trustworthy team of Seismic Retrofit Contractors Los Angeles and surrounding areas that comply with the Los Angeles retrofit requirements and other municipalities in the retrofitting of buildings just like yours. Part 2: Speed of sound, waves, and bedrock. Image credit: J. Louie, University of Nevada-Reno. Outline. Speed of sound. Waves. Bedrock. Urban and wildland environments. Importance for human activities. Kurdistan Region- Iraq. Ministry of Higher Education . & Scientific Research. . Salahaddin. University- Erbil. Geology - 3th Year. 2. nd. Semester . Jan. . 202. 1. Lec.1. 2. Seismic Method . (Applied Seismology).

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